Climatic role of terrestrial ecosystem under elevated CO 2 : a bottom-up greenhouse gases budget
The net balance of greenhouse gas (GHG) exchanges between terrestrial ecosystems and the atmosphere under elevated atmospheric carbon dioxide (CO ) remains poorly understood. Here, we synthesise 1655 measurements from 169 published studies to assess GHGs budget of terrestrial ecosystems under elevat...
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Veröffentlicht in: | Ecology letters 2018-07, Vol.21 (7), p.1108-1118 |
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creator | Liu, Shuwei Ji, Cheng Wang, Cong Chen, Jie Jin, Yaguo Zou, Ziheng Li, Shuqing Niu, Shuli Zou, Jianwen |
description | The net balance of greenhouse gas (GHG) exchanges between terrestrial ecosystems and the atmosphere under elevated atmospheric carbon dioxide (CO
) remains poorly understood. Here, we synthesise 1655 measurements from 169 published studies to assess GHGs budget of terrestrial ecosystems under elevated CO
. We show that elevated CO
significantly stimulates plant C pool (NPP) by 20%, soil CO
fluxes by 24%, and methane (CH
) fluxes by 34% from rice paddies and by 12% from natural wetlands, while it slightly decreases CH
uptake of upland soils by 3.8%. Elevated CO
causes insignificant increases in soil nitrous oxide (N
O) fluxes (4.6%), soil organic C (4.3%) and N (3.6%) pools. The elevated CO
-induced increase in GHG emissions may decline with CO
enrichment levels. An elevated CO
-induced rise in soil CH
and N
O emissions (2.76 Pg CO
-equivalent year
) could negate soil C enrichment (2.42 Pg CO
year
) or reduce mitigation potential of terrestrial net ecosystem production by as much as 69% (NEP, 3.99 Pg CO
year
) under elevated CO
. Our analysis highlights that the capacity of terrestrial ecosystems to act as a sink to slow climate warming under elevated CO
might have been largely offset by its induced increases in soil GHGs source strength. |
doi_str_mv | 10.1111/ele.13078 |
format | Article |
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) remains poorly understood. Here, we synthesise 1655 measurements from 169 published studies to assess GHGs budget of terrestrial ecosystems under elevated CO
. We show that elevated CO
significantly stimulates plant C pool (NPP) by 20%, soil CO
fluxes by 24%, and methane (CH
) fluxes by 34% from rice paddies and by 12% from natural wetlands, while it slightly decreases CH
uptake of upland soils by 3.8%. Elevated CO
causes insignificant increases in soil nitrous oxide (N
O) fluxes (4.6%), soil organic C (4.3%) and N (3.6%) pools. The elevated CO
-induced increase in GHG emissions may decline with CO
enrichment levels. An elevated CO
-induced rise in soil CH
and N
O emissions (2.76 Pg CO
-equivalent year
) could negate soil C enrichment (2.42 Pg CO
year
) or reduce mitigation potential of terrestrial net ecosystem production by as much as 69% (NEP, 3.99 Pg CO
year
) under elevated CO
. Our analysis highlights that the capacity of terrestrial ecosystems to act as a sink to slow climate warming under elevated CO
might have been largely offset by its induced increases in soil GHGs source strength.</description><identifier>ISSN: 1461-023X</identifier><identifier>EISSN: 1461-0248</identifier><identifier>DOI: 10.1111/ele.13078</identifier><identifier>PMID: 29736982</identifier><language>eng</language><publisher>England</publisher><subject>Carbon Dioxide ; Ecosystem ; Greenhouse Effect ; Greenhouse Gases ; Methane ; Nitrous Oxide ; Soil</subject><ispartof>Ecology letters, 2018-07, Vol.21 (7), p.1108-1118</ispartof><rights>2018 John Wiley & Sons Ltd/CNRS.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c972-2d01f634fd78eb8025bc63ae4e6b5317f81bee1059b3181955966b4b6f4df7783</citedby><cites>FETCH-LOGICAL-c972-2d01f634fd78eb8025bc63ae4e6b5317f81bee1059b3181955966b4b6f4df7783</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/29736982$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Liu, Shuwei</creatorcontrib><creatorcontrib>Ji, Cheng</creatorcontrib><creatorcontrib>Wang, Cong</creatorcontrib><creatorcontrib>Chen, Jie</creatorcontrib><creatorcontrib>Jin, Yaguo</creatorcontrib><creatorcontrib>Zou, Ziheng</creatorcontrib><creatorcontrib>Li, Shuqing</creatorcontrib><creatorcontrib>Niu, Shuli</creatorcontrib><creatorcontrib>Zou, Jianwen</creatorcontrib><title>Climatic role of terrestrial ecosystem under elevated CO 2 : a bottom-up greenhouse gases budget</title><title>Ecology letters</title><addtitle>Ecol Lett</addtitle><description>The net balance of greenhouse gas (GHG) exchanges between terrestrial ecosystems and the atmosphere under elevated atmospheric carbon dioxide (CO
) remains poorly understood. Here, we synthesise 1655 measurements from 169 published studies to assess GHGs budget of terrestrial ecosystems under elevated CO
. We show that elevated CO
significantly stimulates plant C pool (NPP) by 20%, soil CO
fluxes by 24%, and methane (CH
) fluxes by 34% from rice paddies and by 12% from natural wetlands, while it slightly decreases CH
uptake of upland soils by 3.8%. Elevated CO
causes insignificant increases in soil nitrous oxide (N
O) fluxes (4.6%), soil organic C (4.3%) and N (3.6%) pools. The elevated CO
-induced increase in GHG emissions may decline with CO
enrichment levels. An elevated CO
-induced rise in soil CH
and N
O emissions (2.76 Pg CO
-equivalent year
) could negate soil C enrichment (2.42 Pg CO
year
) or reduce mitigation potential of terrestrial net ecosystem production by as much as 69% (NEP, 3.99 Pg CO
year
) under elevated CO
. Our analysis highlights that the capacity of terrestrial ecosystems to act as a sink to slow climate warming under elevated CO
might have been largely offset by its induced increases in soil GHGs source strength.</description><subject>Carbon Dioxide</subject><subject>Ecosystem</subject><subject>Greenhouse Effect</subject><subject>Greenhouse Gases</subject><subject>Methane</subject><subject>Nitrous Oxide</subject><subject>Soil</subject><issn>1461-023X</issn><issn>1461-0248</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><recordid>eNo9kD1PwzAQhi0EoqUw8AeQV4YUn504DhuK-JIqdenAFuz4XIqSurIdpP57AoXe8t7w6D4eQq6BzWGsO-xwDoKV6oRMIZeQMZ6r02Mv3ibkIsZPxoBXJZyTyRhCVopPyXvdbXqdNi0NvkPqHU0YAsYUNrqj2Pq4jwl7OmwtBjou-tIJLa2XlNN7qqnxKfk-G3Z0HRC3H36ISNc6YqRmsGtMl-TM6S7i1V_OyOrpcVW_ZIvl82v9sMjaquQZtwycFLmzpUKjGC9MK4XGHKUpBJROgUEEVlRGgIKqKCopTW6ky60rSyVm5PYwtg0-xoCu2YXxsbBvgDU_kprx9uZX0sjeHNjdYHq0R_LfivgG_U5iTA</recordid><startdate>201807</startdate><enddate>201807</enddate><creator>Liu, Shuwei</creator><creator>Ji, Cheng</creator><creator>Wang, Cong</creator><creator>Chen, Jie</creator><creator>Jin, Yaguo</creator><creator>Zou, Ziheng</creator><creator>Li, Shuqing</creator><creator>Niu, Shuli</creator><creator>Zou, Jianwen</creator><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>201807</creationdate><title>Climatic role of terrestrial ecosystem under elevated CO 2 : a bottom-up greenhouse gases budget</title><author>Liu, Shuwei ; Ji, Cheng ; Wang, Cong ; Chen, Jie ; Jin, Yaguo ; Zou, Ziheng ; Li, Shuqing ; Niu, Shuli ; Zou, Jianwen</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c972-2d01f634fd78eb8025bc63ae4e6b5317f81bee1059b3181955966b4b6f4df7783</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Carbon Dioxide</topic><topic>Ecosystem</topic><topic>Greenhouse Effect</topic><topic>Greenhouse Gases</topic><topic>Methane</topic><topic>Nitrous Oxide</topic><topic>Soil</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Liu, Shuwei</creatorcontrib><creatorcontrib>Ji, Cheng</creatorcontrib><creatorcontrib>Wang, Cong</creatorcontrib><creatorcontrib>Chen, Jie</creatorcontrib><creatorcontrib>Jin, Yaguo</creatorcontrib><creatorcontrib>Zou, Ziheng</creatorcontrib><creatorcontrib>Li, Shuqing</creatorcontrib><creatorcontrib>Niu, Shuli</creatorcontrib><creatorcontrib>Zou, Jianwen</creatorcontrib><collection>Medline</collection><collection>MEDLINE</collection><collection>MEDLINE (Ovid)</collection><collection>MEDLINE</collection><collection>MEDLINE</collection><collection>PubMed</collection><collection>CrossRef</collection><jtitle>Ecology letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Liu, Shuwei</au><au>Ji, Cheng</au><au>Wang, Cong</au><au>Chen, Jie</au><au>Jin, Yaguo</au><au>Zou, Ziheng</au><au>Li, Shuqing</au><au>Niu, Shuli</au><au>Zou, Jianwen</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Climatic role of terrestrial ecosystem under elevated CO 2 : a bottom-up greenhouse gases budget</atitle><jtitle>Ecology letters</jtitle><addtitle>Ecol Lett</addtitle><date>2018-07</date><risdate>2018</risdate><volume>21</volume><issue>7</issue><spage>1108</spage><epage>1118</epage><pages>1108-1118</pages><issn>1461-023X</issn><eissn>1461-0248</eissn><abstract>The net balance of greenhouse gas (GHG) exchanges between terrestrial ecosystems and the atmosphere under elevated atmospheric carbon dioxide (CO
) remains poorly understood. Here, we synthesise 1655 measurements from 169 published studies to assess GHGs budget of terrestrial ecosystems under elevated CO
. We show that elevated CO
significantly stimulates plant C pool (NPP) by 20%, soil CO
fluxes by 24%, and methane (CH
) fluxes by 34% from rice paddies and by 12% from natural wetlands, while it slightly decreases CH
uptake of upland soils by 3.8%. Elevated CO
causes insignificant increases in soil nitrous oxide (N
O) fluxes (4.6%), soil organic C (4.3%) and N (3.6%) pools. The elevated CO
-induced increase in GHG emissions may decline with CO
enrichment levels. An elevated CO
-induced rise in soil CH
and N
O emissions (2.76 Pg CO
-equivalent year
) could negate soil C enrichment (2.42 Pg CO
year
) or reduce mitigation potential of terrestrial net ecosystem production by as much as 69% (NEP, 3.99 Pg CO
year
) under elevated CO
. Our analysis highlights that the capacity of terrestrial ecosystems to act as a sink to slow climate warming under elevated CO
might have been largely offset by its induced increases in soil GHGs source strength.</abstract><cop>England</cop><pmid>29736982</pmid><doi>10.1111/ele.13078</doi><tpages>11</tpages></addata></record> |
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language | eng |
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source | MEDLINE; Wiley Online Library Journals Frontfile Complete |
subjects | Carbon Dioxide Ecosystem Greenhouse Effect Greenhouse Gases Methane Nitrous Oxide Soil |
title | Climatic role of terrestrial ecosystem under elevated CO 2 : a bottom-up greenhouse gases budget |
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